2020
Publication Year
2021-01-21T14:38:07Z
Acceptance in OA@INAF
þÿMeasurement of the 154Gd(n,³) cross section and its astrophysical implications
Title
Mazzone, A.; CRISTALLO, Sergio; Aberle, O.; Alaerts, G.; Alcayne, V.; et al.
Authors
10.1016/j.physletb.2020.135405
DOI
http://hdl.handle.net/20.500.12386/29924
Handle
PHYSICS LETTERS. SECTION B
Journal
804
Contents lists available atScienceDirect
Physics
Letters
B
www.elsevier.com/locate/physletb
Measurement
of
the
154
Gd(n,
γ
)
cross
section
and
its
astrophysical
implications
A. Mazzone
a,
b,
S. Cristallo
c,
d,
O. Aberle
e,
G. Alaerts
f,
V. Alcayne
g,
S. Amaducci
h,
i,
J. Andrzejewski
j,
L. Audouin
k,
V. Babiano-Suarez
l,
M. Bacak
e,
m,
n,
M. Barbagallo
e,
a,
V. Bécares
g,
F. Beˇcváˇr
o,
G. Bellia
h,
i,
E. Berthoumieux
n,
J. Billowes
p,
D. Bosnar
q,
A.S. Brown
r,
M. Busso
c,
s,
M. Caamaño
t,
L. Caballero
l,
M. Calviani
e,
F. Calviño
u,
D. Cano-Ott
g,
A. Casanovas
u,
D.M. Castelluccio
v,
w,
F. Cerutti
e,
Y.H. Chen
k,
E. Chiaveri
p,
x,
e,
G. Clai
v,
w,
N. Colonna
a,
G.P. Cortés
u,
M.A. Cortés-Giraldo
x,
L. Cosentino
h,
L.A. Damone
a,
y,
M. Diakaki
z,
M. Dietz
aa,
C. Domingo-Pardo
l,
R. Dressler
ab,
E. Dupont
n,
I. Durán
t,
Z. Eleme
ac,
B. Fernández-Domíngez
t,
A. Ferrari
e,
I. Ferro-Gonçalves
ad,
P. Finocchiaro
h,
V. Furman
ae,
R. Garg
aa,
A. Gawlik
j,
S. Gilardoni
e,
T. Glodariu
af,
K. Göbel
ag,
E. González-Romero
g,
C. Guerrero
x,
F. Gunsing
n,
S. Heinitz
ab,
J. Heyse
f,
D.G. Jenkins
r,
E. Jericha
m,
Y. Kadi
e,
F. Käppeler
ah,
A. Kimura
ai,
N. Kivel
ab,
M. Kokkoris
z,
Y. Kopatch
ae,
S. Kopecky
f,
M. Krtiˇcka
o,
D. Kurtulgil
ag,
I. Ladarescu
l,
C. Lederer-Woods
aa,
J. Lerendegui-Marco
x,
S. Lo Meo
v,
w,
S.-J. Lonsdale
aa,
D. Macina
e,
A. Manna
v,
aj,
T. Martínez
g,
A. Masi
e,
C. Massimi
v,
aj,∗
,
P.F. Mastinu
ak,
M. Mastromarco
e,
p,
F. Matteucci
al,
am,
E. Maugeri
ab,
E. Mendoza
g,
A. Mengoni
v,
w,
V. Michalopoulou
z,
P.M. Milazzo
al,
F. Mingrone
e,
R. Mucciola
v,
aj,
A. Musumarra
h,
i,
A. Negret
af,
R. Nolte
an,
F. Ogállar
ao,
A. Oprea
af,
N. Patronis
ac,
A. Pavlik
ap,
J. Perkowski
j,
L. Piersanti
c,
d,
I. Porras
ao,
J. Praena
ao,
J.M. Quesada
x,
D. Radeck
an,
D. Ramos Doval
k,
R. Reifarth
ag,
D. Rochman
ab,
C. Rubbia
e,
M. Sabaté-Gilarte
x,
e,
A. Saxena
aq,
P. Schillebeeckx
f,
D. Schumann
ab,
A.G. Smith
p,
N. Sosnin
p,
A. Stamatopoulos
z,
G. Tagliente
a,
J.L. Tain
l,
Z. Talip
ab,
A.E. Tarifeño-Saldivia
u,
L. Tassan-Got
e,
z,
k,
P. Torres-Sánchez
ao,
A. Tsinganis
e,
J. Ulrich
ab,
S. Urlass
e,
ar,
S. Valenta
o,
G. Vannini
v,
aj,
V. Variale
a,
P. Vaz
ad,
A. Ventura
v,
D. Vescovi
c,
as,
d,
V. Vlachoudis
e,
R. Vlastou
z,
A. Wallner
at,
P.J. Woods
aa,
R. Wynants
f,
T.J. Wright
p,
P. Žugec
qaIstitutoNazionalediFisicaNucleare,Bari,Italy bConsiglioNazionaledelleRicerche,Bari,Italy cIstitutoNazionalediFisicaNazionale,Perugia,Italy
dIstitutoNazionalediAstrofisica- OsservatorioAstronomicod’Abruzzo,Italy eEuropeanOrganisationforNuclearResearch(CERN),Switzerland
fEuropeanCommission,JointResearchCentre,Geel,Retieseweg111,B-2440Geel,Belgium gCentrodeInvestigacionesEnergéticasMedioambientalesyTecnológicas(CIEMAT),Spain hINFNLaboratoriNazionalidelSud,Catania,Italy
iDipartimentodiFisicaeAstronomia,UniversitàdiCatania,Italy jUniversityofLodz,Poland
kIPN,CNRS-IN2P3,Univ.Paris-Sud,UniversitéParis-Saclay,F-91406OrsayCedex,France lInstitutodeFísicaCorpuscular,CSIC- UniversidaddeValencia,Spain
mTechnischeUniversitätWien,Austria
nCEASaclay,Irfu,UniversitéParis-Saclay,Gif-sur-Yvette,France oCharlesUniversity,Prague,CzechRepublic
pUniversityofManchester,UnitedKingdom
qDepartmentofPhysics,FacultyofScience,UniversityofZagreb,Croatia
*
Correspondingauthorat:DipartimentodiFisicaeAstronomia,UniversitàdiBologna,Italy.E-mailaddress:Cristian.Massimi@bo.infn.it(C. Massimi).
https://doi.org/10.1016/j.physletb.2020.135405
0370-2693/©2020TheAuthor(s).PublishedbyElsevierB.V.ThisisanopenaccessarticleundertheCCBYlicense(http://creativecommons.org/licenses/by/4.0/).Fundedby SCOAP3.
2 A. Mazzone et al. / Physics Letters B 804 (2020) 135405
rUniversityofYork,UnitedKingdom
sDipartimentodiFisicaeGeologia,UniversitàdiPerugia,Italy tUniversityofSantiagodeCompostela,Spain
uUniversitatPolitècnicadeCatalunya,Spain
vIstitutoNazionalediFisicaNucleare,SezionediBologna,Italy
wAgenzianazionaleperlenuovetecnologie,l’energiaelosviluppoeconomicosostenibile(ENEA),Bologna,Italy xUniversidaddeSevilla,Spain
yDipartimentodiFisica,UniversitàdegliStudidiBari,Italy zNationalTechnicalUniversityofAthens,Greece
aaSchoolofPhysicsandAstronomy,UniversityofEdinburgh,UnitedKingdom abPaulScherrerInstitut(PSI),Villigen,Switzerland
acUniversityofIoannina,Greece
adInstitutoSuperiorTécnico,Lisbon,Portugal
aeJointInstituteforNuclearResearch(JINR),Dubna,Russia
afHoriaHulubeiNationalInstituteofPhysicsandNuclearEngineering(IFIN-HH),Bucharest,Magurele,Romania agGoetheUniversityFrankfurt,Germany
ahKarlsruheInstituteofTechnology,CampusNorth,IKP,76021Karlsruhe,Germany aiJapanAtomicEnergyAgency(JAEA),Tokai-mura,Japan
ajDipartimentodiFisicaeAstronomia,UniversitàdiBologna,Italy ak
IstitutoNazionalediFisicaNucleare,SezionediLegnaro,Italy alIstitutoNazionalediFisicaNazionale,Trieste,Italy amDipartimentodiFisica,UniversitàdiTrieste,Italy
anPhysikalisch-TechnischeBundesanstalt(PTB),Bundesallee100,38116Braunschweig,Germany aoUniversityofGranada,Spain
apUniversityofVienna,FacultyofPhysics,Vienna,Austria aqBhabhaAtomicResearchCentre(BARC),India arHelmholtz-ZentrumDresden-Rossendorf,Germany asGranSassoScienceInstitute,L’Aquila,Italy atAustralianNationalUniversity,Canberra,Australia
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Articlehistory:
Received4February2020
Receivedinrevisedform30March2020 Accepted31March2020
Availableonline3April2020 Editor:D.F.Geesaman
Keywords:
sprocess
154Gd
Neutrontimeofflight n_TOF
Theneutroncapturecrosssectionof154Gdwasmeasuredfrom1eVto300keVintheexperimentalarea located185mfromtheCERNn_TOFneutronspallationsource,usingametallicsampleofgadolinium, enrichedto67% in154Gd.Thecapture measurement,performedwithfourC
6D6 scintillationdetectors,
hasbeencomplementedbyatransmissionmeasurementperformedattheGELINAtime-of-flightfacility (JRC-Geel), thus minimising the uncertainty related to sample composition. An accurate Maxwellian averagedcapturecrosssection(MACS)wasdeducedoverthetemperaturerangeofinterestforsprocess nucleosynthesismodelling.Wereportavalueof880(50)mbfortheMACSatkT=30 keV,significantly lowercomparedtovaluesavailableinliterature.Thenewadopted154Gd(n,
γ
)crosssectionreducesthediscrepancy betweenobserved andcalculated solar s-onlyisotopicabundancespredicted bys-process nucleosynthesismodels.
©2020TheAuthor(s).PublishedbyElsevierB.V.ThisisanopenaccessarticleundertheCCBYlicense (http://creativecommons.org/licenses/by/4.0/).FundedbySCOAP3.
1. Introduction
Alltheelementsheavierthanthoseintheirongroup are pro-ducedby a sequence ofneutron capture reactions and
β
decays takingplaceina hotstellar environment,during differentphases ofstellarevolution.Thetwomainprocessesinvolvedaretheslow (s)andtherapid(r)neutroncaptureprocesses.Thesprocess[1,2] owesits nametotheneutron-capture timescale,whichallowsβ
decaytooccur betweenconsecutivecaptureevents.Consequently, aseriesofthesereactionsproducestableisotopesbymovingalong theβ
-stability valley.On theother hand,whenthe neutron den-sitiesarehighenough[3], theneutroncapturesequenceismuch fasterthantheβ
decaysandthepath,therprocesspath,can pro-ceedtoward many short-lived isotopes, approaching the neutron dripline.Mostnuclei receive a contributionfrom both the s andthe r processes(seee.g.[4]).However,afewisotopescannotreceiveany contributionfromtherprocess becausetheyareshieldedagainst
β
decays by stable isobars and for this reason are called s-only isotopes. This is the case of the two gadolinium isotopes 152Gd and 154Gd which are shielded against theβ
-decay chains from the r-process region by their stable samariumisobars, as shown inFig.1.Tobeprecise,152Gdmayreceiveanadditionalcontribu-tionfromthep process,whichproceedsvia photo-disintegration.
Fig. 1. The yellowlinerepresentsthemains-processpathintheSm-Eu-Gdregion; thes-onlyisotopesarehighlightedwithayellowdashedbox.Stableelementsare inblack,β+,β−andβ+radioisotopesareinorange,blueandred,respectively.
Theamountofthep-processcontributiontothe152Gdabundance isstillfarfrombeingpreciselydetermined(see[5] andreferences therein),whileaminorp-processcontributiontothe154Gd
abun-dancecannotbeexcludedaswell.
The almostpure s-processoriginof154Gd(asforother s-only isotopes),makesitscapturecrosssectioncrucialfortestingvarious stellar models aimingatunderstanding s process nucleosynthesis in AsymptoticGiant Branch(AGB) stars,themostimportant
stel-larsiteforthesprocess.Inparticular,relevanthintsontheshape andextensionofthemainsprocessneutronsource,theso-called
13C pocket [6], can be derived. Recently, several studies [7,8,4]
have been conducted analyzing the solar s process abundances in the framework of a Galactic Chemical Evolution (GCE) model toinvestigatetheeffectofdifferentinternalstructures ofthe 13C pocket,whichmayaffecttheefficiencyofthe13C(
α
,n)16Oreaction. In addition, Trippella and Collaborators [9] carried out a similar analysis based on single stellar models. Cristallo et al. [8] and Prantzos et al. [4] have obtained an under-production (-30%) of the154Gd1 s-onlynucleuscomparedto thes-only isotope150Sm, whichisan un-branched isotope,usually assumedasareference for the s process flow. This result is at odds with observations. The authors ofref. [8], have suggested that part ofsuch a devi-ationcould be connectedto uncertainties intheadopted nuclear physicsinputs,takenfromtheKarlsruheAstrophysicalDatabaseof NucleosynthesisinStars(KADoNiS) version0.3 [10],includingthe neutroncapture cross section of 154Gd. In the work by Trippellaetal. [9],problemsforthesprocessproductionofGdwerefound aswell,although inthiscase,thediscrepancybetweenthe abun-dancesof150Smand154Gdislesspronounced.Theneedforanew 154Gd(n,
γ
)measurementwasunderlinedbytheunreasonablepre-dictionforthe over-productionsof152Gdand154Gdwithrespect to their solar abundances. In particular, the ratio 154Gd/152Gd), turnedout tobelower thanunity, whileitisthoughtthat 152Gd should exhibit a higher p-process contribution as compared to
154Gd [9]. In addition, 154Gd was found to be produced
insuffi-cientlycomparedtothelighters-only148Sm and142Nd,produced mostlybythesprocessandpossiblypartlybythepprocess.
Theclose correlationbetweenstellar abundances andneutron capturecross sections calls foran accurate determination of the
154Gd(n,
γ
) crosssection. In addition,thereduction oftheuncer-taintyrelatedto nuclearphysics inputscouldrule outone ofthe possiblecausesofpresentdiscrepancies betweenobservationand modelpredictions oftheabundances. Infact,refinedstellar mod-els requirea full set ofMaxwellian AveragedCapture Cross Sec-tion (MACS) forthermal energies in the range kT
=
8−
30 keV. In the case of 154Gd, 80% of the MACS at kT=
8 keV isdeter-mined bythe capturecrosssection in theneutron energyregion between2
.
7−
300 keV- hereafter werefertothisenergyregion asUnresolvedResonanceRegion(URR).AtkT
=
30 keV,theMACS dependsalmost entirelyon the cross section in the URR. In this energyregion, threetime-of-flight 154Gd(n,γ
) cross sectionmea-surementsarereportedinliterature,byShorinetal.[11],Beerand Macklin[12] andWisshaketal.[13].Theyall covertheURR and therespectiveMACSexhibit largedifferencesandat
kT
=
30 keV, theyrangefrom878(27)mbto1278(102)mb.Therefore,thedata presentintheliterature,sofar,arenotconclusiveenoughto con-strainstellarmodelcalculations.The large spread in the available experimental data could be relatedtothecorrectionsforisotopicimpuritieswhichare neces-sarilyapplied in thedata analysis. Inparticular, the poor knowl-edge oftheir cross sections,given the low naturalabundance of
154Gd(2.18%).Differentdiscrepanciesmayberelatedto:
i) the
de-tectorsusedin thepast experiments,which insome cases could havesuffered from highneutron sensitivity;ii) the experimental determinationofthe neutronflux,whichmighthavebeenbiased insomeprevious measurements;iii) the qualityofoxidesamples andtheneedofcanningforthecontainertoavoidlossofmaterial. Thepresentmeasurementreducedtheimpactoftheselimiting factors,byusingthewell-established,lowneutron-sensitivityC6D6
detectors[14], combined toa self-sustaining metallic sample
en-1 Inthefollowing,anindividualisotopeor/anditsabundanceisimplyindicated
bythesymbol(e.g.152Gd),tosimplifythenotation.
richedin154Gd,andexploitingtheresultsoftherecent155Gd(n,
γ
)measurementperformedatn_TOF[15].Moreover,thegadolinium sample was characterisedby a transmission measurement atthe neutrontime-of-flightfacilityGELINAatEC-JRC-Geel(Belgium).
2. Measurements
Theneutroncapturecrosssectionmeasurementwasperformed attheneutron time-of-flightfacilityn_TOFatCERN.In this facil-ity, neutrons are produced by spallation reactions induced on a leadtargetby20GeV/cprotonsfromtheCERNProtonSynchrotron (PS),whichprovidesatotalof2
×
1015neutrons/pulse,generated by a 7×
1012 protons/pulse primary beam. The initially fastneu-tronsaremoderatedandthencollimatedthroughtwoflightpaths of differentlengths. The presentmeasurement was performedat the experimental area located 185 m from the spallation target. Thislongflight-path,combinedwiththe7nswidthoftheproton bunches from the PS, results in a high energy resolution rang-ing from
E
/
E=
3×
10−4 at 1 eV toE
/
E=
3×
10−3 at 100 keV(calculated usingtheFWHMof theresolutionfunction [16]). Theneutroncaptureeventswereobservedviathedetectionofthe promptγ
-raycascadefrom155Gdexcitedstates.FourC6D6detec-tors, modified forminimizing their neutronsensitivity [14],were arrangedat125◦ relativetotheneutronbeamdirectionandabout 10cmupstreamfromthegadoliniumsampleposition.This config-urationminimisedtheeffectofanisotropicemissionof
γ
cascades whilereducingthebackgroundfromin-beamphotonsscatteredby the sample. The Total Energy detectors (see [17] and references therein) were used in combination with Pulse Height Weighting Technique(PHWT)[18,17].The sample consisted of 0.263 g of metallic gadolinium en-richedat66.78% in 154Gd. Themaincontaminant, i.e.155Gd,was declared by the sample providerat 17.52%. Adetailed resonance analysisofthecapturedata,basedontherecentresultsobtained bytimeofflighton155Gd(n,
γ
)atn_TOF,allowedustoestimatea contentof155Gdequalto20.2%.Thishighervaluewas confirmed byatransmissionmeasurementonthesamesamplecarriedoutat GELINA.AAusample ofthesamediameterwas usedtonormalisethe measured yield, by applying the saturated resonance technique [19]. Also, two other samples with the same diameter of 3 cm wereused.Aleadsampleenabledtheestimateofthebackground, whileanaturalgadoliniumsampleallowedtoassignobserved res-onancestothecorrectgadoliniumisotope,besidesconfirming the isotopiccontentof154Gdintheenrichedsample.
Asmentioned above,thegadoliniumsample was further stud-ied through the transmissionmeasurement ata 10-m station of the GELINA facility. The transmission, T , which was experimen-tally obtained fromthe ratio of Li-glass spectra resulting froma sample-in anda sample-out measurement,is relatedto thetotal crosssection
σ
tot bytheequation:T(En
)
=
e−nσtot(En),
(1)where
n
= (
1.
431±
0.
006)
×
10−4 atoms/bdenotesthearealden-sity ofthegadolinium sample. GELINAis particularlysuitable for high-resolution transmission measurement, because of its time characteristic and the small dimensions of the neutron produc-ing target.Forthisexperiment,the neutronbeamwascollimated to a diameterof 10 mm atthe sample position andfilters were placednearthesampletoabsorbslowneutronsfromtheprevious neutron-burst and to continuously monitor the background. The neutronbeampassing through thesample was detected bya 6.4 mmthickand76mmwideLi-glassscintillatorenrichedto95%in
6Li.Thedetectorwasplacedat10.86mfromtheneutron
4 A. Mazzone et al. / Physics Letters B 804 (2020) 135405
3. Dataanalysisandresults
The experimental capture yield Yc, i.e. the probability for an incident neutron to be captured in the sample, can be deduced from the measured count rate, corrected for the detection effi-ciency of captureevents. By applyingthe PHWT, the count rate, Cw, is weighted in order to make the detection efficiency inde-pendent of the cascade path and
γ
multiplicity. The weighting functionswerecalculatedsimulatingtheresponseofthefull appa-ratusbyaGEANT4[20] Monte-Carlosimulation.Thecaptureyield canbewrittenas:Y
(
En)
=
NCw
(E
n)
−
Bw(E
n)
(E
n)
(2)
where
N is
a normalisationfactor, Bw istheweighted count rate representingthebackgroundandistheneutronfluximpinging on thesample. The neutron energy
E
n was determined fromthe measured timeofflight usingan effectiveflight pathdetermined fromwell-knownlowenergyresonancesinAu[21].The normalisation factor groups together geometrical factors, such as the area of thesample andits beam-interceptionfactor, thesolid angle subtendedby the captureandflux monitors, and the detection efficiency. It was obtained with the saturated res-onance technique applied to the 4.9-eV resonance in197Au. This
normalisation,basedontheAucapturedata,waswithin1.3% con-sistent withthe normalisation derived froma fit to the capture datausingtheparametersfromthetransmissiondata.
The background,Bw, includesdifferentcontributions:
i)
ambi-ent background, which was determined from a measurement in absence of the neutron beam; ii) the sample-independent back-ground(alsoreferredtoasemptybackground),duetotheneutron beam, which was estimated from a measurement with neutron beamimpinging on an empty sample;iii) the sample-dependent background,eitherduetosample-scatteredneutrons(subsequently capturedin theenvironmental materialandgeneratingγ
-rays in the experimental area) ordue toγ
-rays produced at the spalla-tiontargetandreachingtheexperimentalarea,wheretheycanbe scatteredby thesample intothe detectors.Thisthird component wasestimatedbya measurementwithaleadsample inthe neu-tron beam. Previous measurements and Monte-Carlo simulations showedthat thecontributionofthein-beamγ
-raybackgroundis relevantonlyinalimitedenergywindowof1-100keV [16]. There-fore, it was possible to disentangle the two sample-dependent backgroundcomponents inthe time-of-flightspectrum measured withthe lead andwiththe gadoliniumsamples, properlyscaled. The neutron background was scaled forthe elastic cross section and the areal density of the gadolinium andlead sample, while theγ
backgroundwas scaled forthe effectiveatomicnumber of gadolinium and lead samples. The same procedure for the esti-mation of thetotal background was adopted inthe study ofthe197Au(n,
γ
)crosssection.Inparticular,intheenergyregionfrom5keVto500keV,wherethiscrosssection isverywell-known (and above200keV,consideredasastandard)thecapturecrosssection fromthisstudyresultedtobeingoodagreementwithevaluations. In Fig. 2the weighted number ofcounts, registered withthe
154Gdsample, are shown together with the sample-independent
(empty)backgroundandthe sample-dependentbackground com-ponents.Theempty-samplebackgroundcomponentdominatesthe total backgroundover the energyregion of interest,whereas the sample-dependentbackgroundcontributesby lessthan 4% tothe totalbackground.The absolutemagnitudeofthe backgroundwas additionallyverifiedwithdedicatedrunsusingblackresonance fil-ters [17] andafairagreementwasfound.Intheregionbetween5 and300keV,thesignal-to-totalbackgroundratiois2.5.Although the total background level is significant, its uncertainty is small
Fig. 2. Weighted spectrummeasuredwiththe154Gdsamplecomparedtothe
back-groundmeasured with an empty-sampleholderand the one estimatedfrom a measurementwithaleadsample.Thelastspectrumwasobtainedbyscalingthe in-beam
γ
-raybackgroundandthecomponentduetotheneutronsscatteredby thesample,seetextfordetails.Fig. 3. Measured captureyieldandtransmissionofforn+154Gd.Experimentaldata
areshownbyredsymbols,then_TOFR-matrixfitinblueandtheyieldcalculated fromENDF/B-VIII.0parametersingreen,bothincontinuouslines.
since thebackground isdominatedby theempty-sample compo-nent,whichisknownwithin1%.
Theneutronfluxwasevaluatedwithadedicatedmeasurement campaignusingdifferentdetectionsystemsandwithneutroncross section standards [22]. The estimated systematic uncertainty on the flux determination was within 1% below 3 keV [22] and of 3.5% upto300keV.
Intheenergyregionupto2.7keV- hereafterreferredtoas Re-solved Resonance Region(RRR) -,the experimental capture yield was analysed with the Bayesian R-matrix analysis code SAMMY [23].The code can manage experimental effects such asDoppler andresolutionbroadening,self-shieldingandmultipleinteractions of neutrons in the sample. Sizable discrepancies were found for some neutronresonances compared to the yields obtained using theENDF/B-VIII.0evaluationdataset[24].Thesedifferenceswere furtherconfirmedbythetransmissiondata.Anexampleisshown in Fig. 3, where the present results of resonance shape analysis arecomparedtotheexpectedvaluesobtainedusingresonance pa-rametersfromtheevaluateddataset.Upto2.75keV,weanalysed 156 resonances and 3 new resonances were found at 183.17(2), 197.65(1) and 376.26(1) eV, respectively. The statistical analysis of resonance parameters (similar to ref. [15]) yielded a neutron strength function S0
=
2.
78(
33)
×
10−4, an average levelspacingFig. 4.154Gd(n,γ) crosssectionfromthepresentstudycomparedtoprevious
mea-surements(colouredsymbols)andevaluation(continuousline).TheHFcalculation hasbeennormalisedbyafactor0.737(seetext).
Abovethisenergyregion, theexperimental resolution became toolowtoresolveindividualresonancesandanaveragedcross sec-tionwas determinedintheneutronenergyrangefrom2.7keVto 300keV. The captureyield was correctedfor multiple scattering and self-shielding through Monte-Carlo simulations as described inref. [25].Theresultingcorrectionforthetwoeffectswas lower than2%.
Thecontributionofthecontaminantspresentinthemeasured sampleswastakenintoaccountintheexperimentaldataanalysis. In particular, for the main contaminant 155Gd, the cross section
was assumed from the previous n_TOF measurement on 155Gd. In Fig. 4, the capture cross section extracted from this study is comparedtothedataofShorinetal. [11],BeerandMacklin [12], Wisshaketal. [13] andtheENDF/B-VIIIevaluation.IntheURR,the presentdatafairly agreewiththe databy BeerandMacklin[12] andthey are substantially lower than thedata reported by Wis-shak etal.[13] and Shorin etal.[11].This comparisonseems to indicatethat the resultsobtained fromthiswork andby Beeret al.withthesametechnique areinfairagreement,whilethey are inconsistentwiththeresultsbyWisshaketal.andShorinetal. Al-thoughtheselatterdatacomefromasimilarexperimental setup, whereneutronareproducedviathe7Li(n,p)reaction,theneutron flux is normalised to 197Au(n,
γ
) and the capture eventsarede-tectedwith large-volumedetectors, their resultsare inconsistent. AsdiscussedaboveintheIntroduction,thediscrepanciesmightbe relatedtoa problemwiththeneutronsensitivityofthedetectors ortotheexperimentaldeterminationoftheneutronflux.
MACSasa function ofthe thermalenergykT were calculated from the present capture data in the RRR and in the URR. The crosssectionintheenergyregionabovethisrange(i.e.above300 keV)was takenintoaccount by calculationsperformedusingthe HauserFeshbach(HF)statisticalmodeltheory,asimplementedin theTALYScode [26]. Theaverage resonanceparameters,obtained inthepresentanalysisoftheRRR,were constrainedtobe repro-ducedby the calculationsby adjusting the level densityand the
γ
-raystrengthfunction.Anoverallnormalisationbyafactor0.737 oftheresultingcapturecrosssectionwas stillnecessaryto repro-ducethepresentexperimentalMACSatkT
=
30 keV.Theuncertainty onthe MACS takesinto account the uncorre-lateduncertaintyattributabletocountingstatisticsandsystematic uncertainties.Theuncertaintycomponentsoriginatefromthe nor-malisationofthecapturedataandthePHWT(1.3%),theshapeof theneutronflux(1% below3keVand3.5% above)andthe subtrac-tionofthe background(on average2%, depending on theenergy region.). Anotherminor uncertainty is associated withthe align-mentofthesampleanditsgeometricalshape.Asaresult,overthe thermalenergyrangeofkT
=
5−
100 keV,theuncertaintyonthe MACSrangesbetween5and7%.InTable1,thepresentMACSareTable 1
MaxwellianAveragedCaptureCross(inmb)calculatedfor then_TOFdataintheenergyrangekT=5−100 keV.The valuesarecomparedwiththosereportedintheliterature byKADoNiS0.3andKADoNiS1.0.
Energy n_TOF KADoNiS KADoNiS
(keV) 0.3 1.0 5 2160(90) 2801 2947(190) 8 1820(80) – 2195(87) 10 1590(80) 1863 1924(61) 15 1270(80) 1477 1537(33) 20 1080(60) 1258 1326(24) 25 970(50) 1124 1188(19) 30 880(50) 1028(12) 1088(16) 40 770(40) 898 950(14) 50 690(40) 810 856(12) 60 640(40) 745 786(12) 80 560(30) 653 690(15) 100 510(30) 591 626(19)
reportedforthethermalenergygridproposedbyKADoNiS[10,27]. In the whole energy range,the MACS valuesfrom our measure-mentaresignificantlylowerthanKADoNiS.Itisinterestingtonote thatthedisagreementworsenedwiththenewversionofthe eval-uation,thedeviationbeingbetween10% and20%.
4. Astrophysicalimplications
As discussed above, a new determination of the 154Gd neu-troncapturecrosssectionwasmotivatedbyadiscrepancybetween stellar models and observations, as highlighted by [8] and con-firmed by [4], where a lower theoretical 154Gd/150Sm ratio with respect to that measured in the Sun (and derived forthe early-solarsystem)wasfound.Infact,theoreticalvalues,whichinclude yields fromtheAsymptotic GiantBranch(AGB) phaseoflow and intermediate massstars (takenfromthe FRUITYdatabaseofAGB starnucleosynthesis[28,29]),show an under-productionof154Gd withrespectto150Sm:154Gd/150Sm=0.70.Asaconsequence,one
canarguethatareasonforthedisagreementshouldbeattributed toproblemsinthecrosssectionof154Gditself.
Theuseofthepresentcrosssectionleadstoanincreaseofthe theoreticalsolar154Gdabundanceby10%onaverage.2 The differ-ence in the 154Gd surface abundances is lower than the change
of the neutroncapture crosssections (on average 15% compared toKaDoNiS0.3).Thisisbecausethe154Gdproduction/destruction
strongly depends on the branching at 154Eu, which is an unsta-ble isotope (its decay lifetime in the terrestrial condition is 8.6 y).Thisbranchingisby-passedwhenthemajorneutronsourcein AGB stars(the 13C(
α
,n)16Oreaction) isactivated,duetoits short lifetime forthe timescale characterizing neutroncaptures in this regime.Thesituationmaybedifferentduringthermalpulseswhen thehighertemperaturecanefficientlyactivatethe22Ne(α
,n)25Mgneutronsource(which producesa definitelyhigherneutronflux). In such a case, the neutron capturechannel is competitive com-pared to the
β
decay channel and, as a consequence, the main s-processpath may by-pass 154Gd. The delicate balance between neutron captures on 154Gdandβ
decays from 154Eu determinesthefinalabundanceof154Gd.
In summary,the presentexperimental value leads toa better agreementbetweenmodelcalculationsandobservations,although itisnotabletocompletelyremovethemismatch.In2009,Lodders andcollaborators [30] estimatedtheuncertaintyinthe determina-tion of the solar gadolinium3 abundance to be
±
15% (and±
5%2
NotethatonlyalimitednumberofAGBmodelshavebeeninvestigatedwith thepresentcrosssection.TheevaluationoftheeffectinafullGCEmodelwillbe publishedseparately.
6 A. Mazzone et al. / Physics Letters B 804 (2020) 135405
forsamarium).Theadoptionofthepresent154Gdneutroncapture
crosssection,eventuallyleadstoanew154Gd/150Sm ratioof0.77 inFRUITYmodels.Whentakingintoconsiderationthelowerlimit of the present neutron capture cross section, we obtain 154Gd/ 150Sm
0.81. As a consequence, the ratios obtained in FRUITY
modelsarenowcompatiblewiththeobservedabundances,within observationaluncertainties(
±
20%).Whenthepresentcrosssectionisusedinthemodelsby Trip-pellaetal. [9,31],itisinterestingtonoticethatwhilethe discrep-ancywithrespectto142Nd,148Smand152Gdiscompletelyerased
(duetothelargerproductionof154Gd),atthesametime, the
ra-tio154Gd/150Smattainsavalue(1.15)consistentwithobservations, within uncertainties. In general, it appears that the approach in ref. [31] produces a flatter distribution of s process isotopes, al-though this was obtained in post-process computations and not infullstellarmodels.Therefore,aclearsuggestionemergingfrom thepresent154Gd(n,
γ
)crosssectionmeasurementisthatsomeoftheremainingmodelambiguitiesmightbesolvedbyamergingof themixingapproachespresentedinFRUITYandref. [9],something thatisinanadvancedstageofimplementation[32].
Anotherimportant outcome fromthiscombined experimental and theoretical study is related to the 154Gd abundance, which largelydependsonthebranchingat154Eu.Forthisisotope,no
ex-perimental dataare available for both the neutron capturecross section and the temperature-dependent
β
decay rate. Therefore, sprocess calculationsarebased onpurely theoreticalestimations (seeref. [33] andref. [34],respectively). Alower 154Eu(n,γ
) crosssection or a faster 154Eu(
β
−)154Gddecay would lead to a larger154Gdsurface abundance withrespect to 150Sm (andvice-versa).
Therefore,thepresentresultsuggeststhatadditionaleffortsshould be spent inthisdirectionfrom theexperimental side, to provide experimentalvaluesasdetailedaspossibletostellarmodellers.
Declarationofcompetinginterest
Theauthorsdeclarethattheyhavenoknowncompeting finan-cialinterestsorpersonalrelationshipsthatcouldhaveappearedto influencetheworkreportedinthispaper.
Acknowledgements
The isotopeused in thisresearch was supplied by theUnited StatesDepartmentofEnergyOfficeofSciencebytheIsotope Pro-gramintheOfficeofNuclearPhysics.
This research was supported by the EUFRAT open access pro-grammeoftheJointResearchCentreatGeel.
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